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One-Dimensional Consolidation of Unsaturated Soil Deposit with Various Initial Conditions

机译:不同初始条件下非饱和土的一维固结

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This study presents a novel analytical solution for one-dimensional (1-D) consolidation for unsaturated soils using the Eigen function expansion method to solve inhomogeneous governing equations of air and water phases. Eigen functions and eigenvalues are parts of the general solution and can be obtained based on the proposed boundary condition. Additionally, the Laplace transform method is adopted to solve the first-order differential equations. Once equations with transformed domain are all obtained, the final solutions, which are proposed to be functions of time and depth, can be achieved by taking an inverse Laplace transform. The mathematical procedure accentuates a non-uniform initial condition, in which initial excess pore pressures are linearly decreasing with depth. Dimensionless parameters λ_a and λ_w that control the gradients of distributions of initial excess pore-air and pore-water pressures, respectively, are introduced in this paper. A worked example is provided to investigate effects of λ_a and λ_w on the consolidation behaviour of unsaturated soils.
机译:这项研究提出了一种新的解析方法,该方法使用特征函数展开法求解不饱和土壤的一维(1-D)固结气固两相控制方程。特征函数和特征值是一般解的一部分,可以根据所提出的边界条件获得。另外,采用拉普拉斯变换法求解一阶微分方程。一旦获得了所有具有变换域的方程,就可以通过进行拉普拉斯逆变换来获得最终的解决方案,该解决方案被建议为时间和深度的函数。数学过程强调了一个不均匀的初始条件,其中初始过量孔隙压力随深度线性减小。介绍了分别控制初始过剩孔隙空气压力和孔隙水压力分布梯度的无量纲参数λ_a和λ_w。提供了一个工作实例来研究λ_a和λ_w对非饱和土固结特性的影响。

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